airborne technologies for disaster management · 2019-08-28 · airborne technologies for disaster...
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AIRBORNE TECHNOLOGIES FOR DISASTER MANAGEMENT
Jürgen Schulz
Hansa Luftbild AG, 48147 Münster, Germany, [email protected]
KEY WORDS: airborne remote sensing, flooding, urban flash floods, bark beetle
ABSTRACT:
Currently, satellite-based systems and UAVs are very popular in the investigation of natural disasters. Both systems have
their justification and advantages - but one should not forget the airborne remote sensing technology. The presentation shows
with three examples very clearly how airborne remote sensing is still making great progress and in many cases represents the
optimal method of data acquisition.
The airborne detection of forest damages (especially currently the bark beetle in spruce stands) can determine the pest attack
using CIR aerial images in combination with ALS and hyperspectral systems - down to the individual tree. Large forest areas
of 100 sqkm and more can be recorded from planes on one day (100 sqkm with 10cm GSD on one day).
Flood events - such as on the Elbe in 2013 - were recorded by many satellites. However, many evaluations require high-
resolution data (GSD 10cm), e.g. to clarify insurance claims. Here the aircraft system, which was able to fly below the cloud
cover and was constantly flying at the height level of the flood peak, proved to be unbeatable.
The phenomenon of urban flash floods is one of the consequences of climate change. Cities are not in a position to cope with
the water masses of extreme rain events and so are confronted with major damages. In Germany, a number of cities are
already preparing to manage short-term but extreme water masses. The complicated hydrographic and hydraulic calculations
and simulations require above all one thing - a precise data basis. This involves, for example, the height of kerbstones and the
recording of every gully and every obstacle. Such city-wide data can only be collected effectively by photogrammetric
analysis of aerial photography (GSD 5 to 10cm).
1. INTRODUCTION
Airborne remote sensing has a long tradition in which
Hansa Luftbild played a decisive role. Founded in 1923,
Hansa Luftbild quickly became the largest aerial
photography company in the world, flying through
Antarctica, Greenland, Afghanistan, China and Peru. A
mountain range in the Antarctic is still named after the
pilot of Hansa Luftbild "Bundermann Chain".
Fig 1: Hansa Luftbild Photograph Fig 2: Bundermann Chain (Antarktis)
Max Bundermann
Today, Hansa Luftbild is a leading European company in
the fields of airborne remote sensing, photogrammetry,
laser scanning and geodata processing - however, due to
technical developments and the competitive situation, this
position has to be constantly redefined.
According to an increasing number of technical articles,
airborne remote sensing will soon be replaced by satellite
data and drones. In fact, there is enormous technical
progress in satellites and drones, so such an assessment
seems realistic. But is the importance of airborne geodata
acquisition really diminishing - or is it even becoming
superfluous?
A brief comparison of the systems with regard to the
topic of "disaster management" gives a differentiated
picture.
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLII-3/W8, 2019 Gi4DM 2019 – GeoInformation for Disaster Management, 3–6 September 2019, Prague, Czech Republic
This contribution has been peer-reviewed. https://doi.org/10.5194/isprs-archives-XLII-3-W8-387-2019 | © Authors 2019. CC BY 4.0 License.
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Satellite data have a big advantage - the satellite orbits
the earth and can capture virtually any location (or
disaster). If it is a satellite family, disasters can be
identified very shortly after their occurrence and
measures to save human lives can be supported at short
notice. There are already many examples of this,
including earthquake disasters and floods. On the other
hand, there are serious disadvantages - you fly above the
cloud cover, which optical sensors cannot penetrate.
Another disadvantage is the geometric resolution. A high
resolution (currently 30cm) is very expensive due to the
commercialization of satellite remote sensing. With its
Copernicus program, the European Union offers an
important alternative - the data are free of charge, but
currently with resolutions of 10 meters at Sentinel-2.
Relatively low flying drones seem to be the solution to
capture the extent of a disaster with high detailing. The
current development of the drones and their sensors is
breathtaking. Optical sensors, laser scanners and
hyperspectral technology mounted on drones allow the
highest resolutions and accuracies. There are now so
many providers of the most diverse technical designs of
drones that geo-exhibitions (such as Intergeo in
Germany) effortlessly fill a large hall exclusively with
drones.
However, there are clear limits to the use of drones in
disaster situations. On the one hand, the systems in
question are classified as “aircraft” and are thus subject to
the requirements of the authorities for flight safety as
well as aircraft (application for a permit to fly, etc.).
Furthermore, there are national regulations for the
operation of drones. In Germany, for example, it is not
permitted to operate drones outside the field of vision of
the drone pilot. This significantly limits the coverage of
larger areas. In any case, there are clear limits to the use
of drones in large disaster areas (e.g. floods); the high
time and personnel requirements also lead to high costs.
Satellite data and the use of drones therefore have many
advantages for the collection of geodata in the event of a
disaster - but also very clear disadvantages. Ultimately,
the type, location and extent of the disaster will determine
which data is required. This dialectic of advantages and
disadvantages naturally also applies to the airborne
acquisition of geodata. However, there are a strikingly
large number of applications where the most valuable
information for coping with disasters is provided by
aircraft. From flight altitudes between approx. 200-800
meters the necessary information can be obtained
quickly, comprehensively and up-to-date with a good
accuracy. This compensates for some disadvantages, such
as the relatively high costs. And, unfortunately, cross-
border operations are still very difficult due to the
different legislation and the associated difficulties in
obtaining a permit to fly in a neighbouring country.
Three very different examples will be used in the
following to demonstrate how airborne remote sensing
can achieve optimum results in disaster situations.
2. FLOODS AT RIVERS
In 2013 there was an extreme flood event on one of the
largest German rivers - the Elbe. Caused by heavy
rainfall in the Czech Republic followed by flooding in the
Czech Republic, the peak of the flood reached Germany
at the beginning of June and moved to Hamburg within a
few days only. Large areas along the Elbe, Saale and
Mulde rivers were flooded. An impression is given by
figure 3.
Fig 3: Flooding of river Elbe (taken from Hansa Luftbild airplane)
Hansa Luftbild received the demanding order to record
this damage event by means of aerial photographs.
The decisive challenge was to capture the pictures with a
geometric resolution of 10 cm. At the same time, the
images should always be taken at the peak of the tidal
wave. This set a very narrow time window, i.e. in view of
the – of course - bad weather it was necessary to fly
below the cloud cover.
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLII-3/W8, 2019 Gi4DM 2019 – GeoInformation for Disaster Management, 3–6 September 2019, Prague, Czech Republic
This contribution has been peer-reviewed. https://doi.org/10.5194/isprs-archives-XLII-3-W8-387-2019 | © Authors 2019. CC BY 4.0 License.
388
The task could be solved by using a camera DMC-1
(Zeiss/Intergraph; now Hexagon) mounted on a twin-
engine Cessna-404. In order to achieve a GSD of 10cm
with this camera, a flight altitude of 1000 meters above
ground must be maintained - so that one could mostly
stay under the clouds.
The flood area was huge and stretched from the German-
Czech border South of Dresden to shortly before
Hamburg, supplemented by the floods of the tributaries
Saale and Mulde. The total length was 983 river
kilometres and the area 2,471 square kilometres. 16,693
coloured aerial photos were taken.
date photos region
05.06.2013 2.952 River Mulde
06.06.2013 1.510 River Saale North
07.06.2013 3.086 River Saale South
07.06.2013 1.922 River Elbe South
08.06.2013 591 River Elbe South
09.06.2013 2.992 Elbe and Rosenburg
10.06.2013 1.087 Elbe to Wittenberge
11.06.2013 1.988 Elbe and Fischbeck
12.06.2013 5.65 River Elbe North
16.693
Table 1: Project timeline
The flood areas were so large that many parallel flight
strips were necessary.
Fig 4: Flight planning near Magdeburg (excerpt)
Fig 5: Project area Elbe, Saale and Mulde
The situation was aggravated by two severe dam breaches
(Rosenburg and Fischbeck) during the project. Here the
flight planning had to be changed very quickly so that the
new areas could be recorded at short notice.
Of course the flood was also observed by various
satellites, but optical data with 10cm resolution below the
cloud cover could not be obtained. And for a drone
mission the area was simply much too large.
Image data could thus be obtained under very difficult
conditions - but the decisive factor is how this
information was used for disaster management. For
example, Hansa Luftbild was able to participate in
follow-up projects in which the aerial photographs were
used to precisely define the water-land boundary. In this
way, the aerial photographs served to settle claims for
damages by insurance companies.
But far more important are the hints for the planning of
new protective measures (raising the dike by identifying
weak points in the dike system, designating polder areas,
renaturing water bodies, improving the safety of fuel oil
tanks, etc.).
The evaluation of the data also served to improve cross-
border flood risk management (in this case in particular
the cooperation of German and Czech authorities).
3. URBAN FLASH FLOODS
The second example of airborne disaster management
also has something to do with "too much water", but it
does not announce itself several days before as in the first
example. In the case of so-called urban flash floods (or
heavy rainfall events), water comes out of the clouds in
extreme quantities without prior notice. Climate change
means that we increasingly have short, extreme weather
events - including flash floods of this kind. Cellars and
underground garages that are full to capacity with rain
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLII-3/W8, 2019 Gi4DM 2019 – GeoInformation for Disaster Management, 3–6 September 2019, Prague, Czech Republic
This contribution has been peer-reviewed. https://doi.org/10.5194/isprs-archives-XLII-3-W8-387-2019 | © Authors 2019. CC BY 4.0 License.
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water are very annoying, but in some cases there is also
danger to life and limb.
It is impossible to record such events by satellite, airplane
or drone, because the event often lasts only a few hours
or less. The damage, on the other hand, is enormous,
especially of course if the area is inhabited. Subsequent
damage mapping is of course feasible with remote
sensing. The better way, however, is to provide the
appropriate geoinformation for damage prevention or at
least damage limitation. This enables local authorities to
prepare for such events.
In Germany there are already the first municipalities that
use geodata for protection against urban flash floods. Not
only because they are legally obliged to take precautions,
but also because many municipalities have already had
negative experiences. This includes Münster, Hansa
Luftbild's home town (see Figure 6).
Fig 6: Urban Flash Flood in Münster city Fig 7: Urban Flash Flood,
(Source: dpa/cas fdt) Water in a private house
The key questions with this problem are "Where does the
water flow to?" and "Where does it damage?". This
requires a local, detailed model-based investigation. Such
a simulation requires good input data. Some of these data
should be available in every municipality (building stock,
sewer data, etc.). Other data are not available or of
insufficient quality (elevation model, break lines, etc.).
Figure 8 shows a section of a medium-sized city on the
edge of the Black Forest, which was flown by Hansa
Luftbild in spring 2019 (GSD 5cm, overlaps 60%/50%).
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLII-3/W8, 2019 Gi4DM 2019 – GeoInformation for Disaster Management, 3–6 September 2019, Prague, Czech Republic
This contribution has been peer-reviewed. https://doi.org/10.5194/isprs-archives-XLII-3-W8-387-2019 | © Authors 2019. CC BY 4.0 License.
390
Fig 8: Basic image for a risk map
A digital elevation model (DEM) was generated by a
matching process of the aerial photographs. One can
clearly see that the terrain in the upper part of the image
(North) is higher, so the water will mainly flow from
North to South. However, break lines were also
measured. These show that the water is dammed at the
upper light green east-west road and forced in certain
directions. South of this road there are dark green areas
which represent depressions and thus collect the water.
The residential buildings located there are very
susceptible to flooding. If there is also a kindergarten
underneath, the situation may become dramatic.
It is therefore necessary to provide precise data on the
possible flow paths of the water (i.e. also the height of the
kerbs, the location of each gully, and the detection of
each obstacle).
In addition to the data on the urban sewerage system, this
is all important input information for a hydraulic
simulation. There are numerous commercial programs for
this and there are specialized companies with which
Hansa Luftbild cooperates.
Finally, it is about the production of hazard maps or risk
maps of an urban area, which provide vital information
for urban planning, urban drainage, disaster control and
the public. The data can be used to prevent heavy rainfall,
e.g. by
- construction of drainage ditches and rainwater retention
basins
- unsealing of surfaces or replacement by water-
permeable surface coverings
- erection of obstacles (walls) to force flowing water in
directions
- roof greenings
- keeping areas free for natural infiltration, creating green
areas
Danger of urban flash floods is real and one has to
prepare the protection from them seriously. Good
simulation programs also require good geodata as a basis.
Airborne remote sensing - and apparently only this - can
provide the required accurate geodata.
4. FOREST DAMAGE CAUSED BY BARK
BEETLES
Drought and pest infestation have dramatically worsened
the condition of our forests in recent years. In addition,
there were storms such as the recent storm "Eberhard".
There is no doubt that global climate change is also
increasingly causing extreme weather events that damage
forests, to which forest administrations and forest owners
must respond.
Above all, special attention must urgently be paid to the
rampant bark beetle infestation in order to prevent or at
least limit its further spread. This requires an up-to-date
knowledge of the affected areas, ideally early detection.
The known forest methods (visual terrestrial observation
by forest specialists, pheromone traps, etc.) are currently
reaching their limits and should be supplemented by
detailed information from the air.
The basic advantages of remote sensing become clearly
visible - namely to provide data up-to-date, fast and
homogenously area-wide.
Airborne remote sensing can primarily offer visible and
near infrared airborne surveys. For special applications
the "Airborne Laser Scanning" and the hyperspectral
flights or a combination of these data is useful.
In the summer of 2018 Hansa Luftbild was asked to carry
out a project for the State enterprise “Sachsenforst”, in
which the National Park "Saxon Switzerland" at the
German-Czech border was captured using aerial photos
(10 cm pixels) and digital orthophotos were produced.
The purpose of this inventory was to identify forest areas
damaged by the bark beetle.
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLII-3/W8, 2019 Gi4DM 2019 – GeoInformation for Disaster Management, 3–6 September 2019, Prague, Czech Republic
This contribution has been peer-reviewed. https://doi.org/10.5194/isprs-archives-XLII-3-W8-387-2019 | © Authors 2019. CC BY 4.0 License.
391
Fig 9: Ortho photo National Park „Sächsische Schweiz", obtained and processed by Hansa Luftbild
(reddish: healthy stands; grey: infested stands)
As the photo shows, such areas can be well delimited by
means of visual control. Of course, typical signs of
infestation, such as drilling dust at the base of the trunk,
are not visible in aerial photographs - but crown
discoloration and crown thinning indicate the activity of
the bark beetle and are clearly visible in the aerial
photograph. Particularly in the infrared range (as in the
picture above) the damage picture and - with repeated
flights - the damage process can be represented well and
thus also an early detection is possible. The intersection
of these data with existing information in a GIS (forest
operation maps, forest type maps, ...) supports semi-
automatic screening and infestation detection.
Of course, special flights are correspondingly complex.
On the other hand, 100 sqkm of forest with 10cm pixels
can be captured on a single (cloud-free) day; in the colour
and infrared range with the possibility of single tree
assessment.
For a good damage mapping, image data with at least
20cm resolution are necessary, which again places the
airborne remote sensing in the foreground.
However, the big challenge with the problem "bark
beetle" is its early detection.
In general, the physiological needle changes during pest
infestation are divided into three phases: green, red and
grey. Damage in the red phase (visible discoloration of
the needles) and in the grey phase (few/no needles and
grey trunk) can already be sufficiently detected in the
aerial photograph (see above). The focus is on the
identification of dead trees and the area-related
documentation of damage. However, it is very desirable
to enable early detection of bark beetles already in the
green phase and thus to allow early human intervention.
The transition from the green to the red phase has a very
complex background; there is, however, a well-founded
assumption that disturbances in the pigment balance are
causal and are reflected spectrally. Narrow-band
wavelengths (e.g. at 717 nm) could support a distinction
between "infested" and "uninfected" at an early stage of
beetle infestation.
Airborne hyperspectral sensors offer the possibility to
detect in such specific wavelengths, but the detection of
forest areas is not yet very common. Hansa Luftbild is
cooperating with the Hungarian company Envirosense.
Initial results give reason to hope that hyper spectroscopy
will be used to detect early bark beetle damage.
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLII-3/W8, 2019 Gi4DM 2019 – GeoInformation for Disaster Management, 3–6 September 2019, Prague, Czech Republic
This contribution has been peer-reviewed. https://doi.org/10.5194/isprs-archives-XLII-3-W8-387-2019 | © Authors 2019. CC BY 4.0 License.
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Fig 10: Differentiation of tree types by means of hyper spectroscopy
Figure 10 shows the result of a combined hyperspectral
and laser data evaluation. The images were taken with an
AISA Kestrel10 hyperspectral sensor (1.0m ground pixel)
and a Leica ALS70 laser system (8 points/sqm). The use
of pixel-based and object-based classification programs
allowed the production of a tree species map.
This method is currently being further developed in the
direction of early detection of forest damage. The
hyperspectral method will certainly receive a boost with
the launch of the Copernicus satellite EnMAP next year.
5. SUMMARY
Three selected examples showed that airborne
technologies make valuable and unique contributions to
disaster management.
Despite enormous progress in satellite and drone
technology, this will obviously remain the case for many
years to come.
ACKNOWLEDGEMENTS
The author wishes to thank the State enterprise
Sachsenforst for the permission to use figure 9. The
author also wishes to thank company Envirosense Kft.
(Hungary) for the good cooperation and for the
permission to use figure 10.
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLII-3/W8, 2019 Gi4DM 2019 – GeoInformation for Disaster Management, 3–6 September 2019, Prague, Czech Republic
This contribution has been peer-reviewed. https://doi.org/10.5194/isprs-archives-XLII-3-W8-387-2019 | © Authors 2019. CC BY 4.0 License.
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